(Table S1) Tie-points used in age model construction for ODP Leg 172 sites

• Main Authors: Thornalley, David JR, Barker, Stephen, Becker, Julia, Hall, Ian R, Knorr, Gregor
• Format: Dataset
• Language: English
• Published: PANGAEA 2013
• Subjects: 172-1055; 172-1057; 172-1059; 172-1060; 172-1061; 172-1063; Age model; Blake-Bahama Outer Ridge; North Atlantic Ocean; Blake Outer Ridge; Carolina Slope; COMPCORE; Composite Core; DEPTH; sediment/rock; Elevation of event; Event label; Joides Resolution; Latitude of event; Leg172; Longitude of event; Ocean Drilling Program; ODP; Tie point; North Atlantic; Northwest Atlantic
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.821830; https://doi.org/10.1594/PANGAEA.821830

ix Ocean Drilling Program (ODP) sites, in the Northwest Atlantic have been used to investigate kinematic and chemical changes in the "Western Boundary Undercurrent" (WBUC) during the development of full glacial conditions across the Marine Isotope Stage 5a/4 boundary (~70,000 years ago). Sortable silt mean grain size(sort s) measurements are employed to examine changes in near bottom flow speeds, together with carbon isotopes measured in benthic foraminifera and % planktic foraminiferal fragmentation as proxies for changes in water-mass chemistry. A depth transect of cores, spanning 1.8-4.6 km depth, allows changes in both the strength and depth of the WBUC to be constrained across millennial scale events. Sort s measurements reveal that the flow speed structure of the WBUC during warm intervals ("interstadials") was comparable to modern (Holocene) conditions. However, significant differences are observed during cold intervals, with higher relative flow speeds inferred for the shallow component of the WBUC (~2 km depth) during all cold "stadial" intervals (including Heinrich Stadial 6), and a substantial weakening of the deep component (~3-4 km) during full glacial conditions. Our results therefore reveal that the onset of full glacial conditions was associated with a regime shift to a shallower mode of circulation (involving Glacial North Atlantic Intermediate Water) that was quantitatively distinct from preceding cold stadial events. Furthermore, our chemical proxy data show that the physical response of the WBUC during the last glacial inception was probably coupled to basin-wide changes in the water-mass composition of the deep Northwest Atlantic.